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作 者:钱君龙[1] 柯晓康[1] 王明珠[1] 柯善哲 陈逸君
机构地区:[1]中国科学院南京地理与湖泊研究所
出 处:《南京林业大学学报(自然科学版)》1998年第1期22-26,共5页Journal of Nanjing Forestry University:Natural Sciences Edition
基 金:国家自然科学基金
摘 要:用实测数据阐明了白桦1995年年轮中化学元素钾、锰、铜、锌、锶、镉、钡、铅含量C(Z,t)和根部暗棕壤中对应元素的C′(Z,t)具有相关性,并且满足对数线性相关模式:lgC′(Z,t)=a(Z)+b(Z)lgC(Z,t),其中原子序数Z用于表征不同元素,t是年轮所属的年份,统计系数a、b由线性回归确定。利用相关模式,可由实测的逐年年轮中化学元素含量的年份序列C(Z,t),得到环境(土壤)中化学元素含量的逐年演变C′(Z,t),由C′(Z,t)的最低值可以估算当地表层土壤元素背景值的上限。Three white birch trees growing at shuangling Forei Farm in Heilongjiang province were selected to determine the contents of 8 chemical elements both in the 1995′s growth rings, C(Z、t) , and in the soils near the roots, C′(Z,t) , of the trees. The results showed that the relationship between C(Z,t) and C′(Z,t) followed the logarithmic linear correlation model, lg C′(Z,t) = a(Z)+b(Z) lg C(Z,t) .Where Z is the atomic number of element, and the year when the tree ring grows. Based on this model the chrono sequences of chemical element contents in the soils were reproduced from those in the tree rings; i. e., the dynamic variations in the chemical element contents of the soils at the sites were traced. In this study the chrono sequences of the chemical elements including k, Mn, Cu, Zn, Sr, Cd, Ba and Pb in the soils near the roots of white birch trees from 1954 to 1995 were established, and the background values of K, Mn, Cu, Zn, Sr, Cd, Ba and Pb in the soil were calculated by taking the lowest values of the chrono sequences of the element contents as upper limits of the background values.
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